Premium
Offshore sediment overpressures of passive margins: Mechanisms, measurement, and models
Author(s) -
Dugan B.,
Sheahan T. C.
Publication year - 2012
Publication title -
reviews of geophysics
Language(s) - English
Resource type - Journals
SCImago Journal Rank - 8.087
H-Index - 156
eISSN - 1944-9208
pISSN - 8755-1209
DOI - 10.1029/2011rg000379
Subject(s) - overpressure , geology , pore water pressure , submarine pipeline , petrology , diagenesis , tectonics , hydrostatic equilibrium , consolidation (business) , fluid dynamics , geotechnical engineering , seismology , mineralogy , mechanics , physics , accounting , quantum mechanics , business , thermodynamics
Fluid pressure in excess of hydrostatic equilibrium, or overpressure, in offshore environments is a widespread phenomenon that contributes to the migration and storage of fluids, solutes, and energy and to the potential mechanical instability of these sediments. Overpressure exists in deep and shallow systems and is most likely to be found where low‐permeability (<10 −16 m 2 ) layers have inhibited pore fluid escape or there have been large forcing mechanisms (e.g., rapid sedimentation, tectonic stressing, heating, and volume‐creating reactions). The genesis and magnitude of overpressure can be controlled by physical processes (e.g., rapid sedimentation (>mm/yr), tectonic loading, and lateral fluid transfer) and thermal and chemical processes (e.g., aquathermal expansion, hydrocarbon generation, mineral diagenesis, and organic maturation). In systems where near‐lithostatic overpressures are generated, potentially unstable sediments are created. Failures of these sediments can create large‐scale natural disasters, generate fractures, and damage seafloor and subseafloor infrastructure. Detailed characterization of overpressured systems has been accomplished through geological and geotechnical analyses, including investigation of physical‐mechanical properties (mainly porosity, consolidation state, and shear strength), inversion of geophysical data (e.g., compressional and/or shear velocities), measurement of in situ properties, and postevent analyses. Process‐based models have been developed to explain the origin of overpressure in terms of rate of overpressure genesis. This allows identification of potentially unstable zones and assessment of the potential for failure. Future development in measurements and in coupling of models will lead to more accurate analysis and prediction of fluid pressure in offshore sediments, which in turn will facilitate better hazard analyses and will enable safer and more cost‐effective offshore drilling practices and other offshore infrastructure development.